Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
7450443 | Quaternary International | 2018 | 7 Pages |
Abstract
In the macro-region of study, two types of sources can be differentiated on the basis of their primary location: high-altitude sources emplaced in the Andes range (â¥2500 m a.s.l.) including Laguna del Diamante, Laguna del Maule, and Las Cargas sources; and low-altitude (â¤1500 m a.s.l.) extra-Andean sources situated on the eastern plains: Cerro Huenul and El Peceño. In addition, while the primary location of Arroyo Paramillos source is currently unknown, we consider it as a sub source of Laguna del Diamante, since its wide archaeological distribution has a main core within Laguna del Diamante area and in the upper Maipo River basin. Considering this pattern, the assignation of provenances presented here improves the basis for assessing the use of high Andean environments from both sides of the mountain range. In addition, we will also improve the geochemical discrimination between the two sources Arroyo Paramillos and Las Cargas that based on only previous XRF analysis are chemically overlapping, leading to an incorrect interpretation of their pattern of archaeological distribution. The better characterization of the obsidian sources of the Laguna del Diamante and neighboring regions allows discussions of mobility, exchange, and human use of this lithic resource in the highland of central western Argentina - central Chile.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geology
Authors
Anna Maria De Francesco, Donatella Barca, Marco Bocci, Valeria Cortegoso, Ramiro Barberena, LucÃa Yebra, VÃctor Durán,